Elucidating phosphorus removal dynamics in a denitrifying woodchip bioreactor.

Sci Total Environ

Environmental Research Institute, School of Science, Faculty of Science and Engineering, University of Waikato, Kirikirioa Hamilton, New Zealand; Lincoln Agritech Ltd, Ruakura, Kirikirioa Hamilton 3214, New Zealand. Electronic address:

Published: March 2024

Denitrifying woodchip bioreactors (DBRs) are an established nitrate mitigation technology, but uncertainty remains on their viability for phosphorus (P) removal due to inconsistent source-sink behaviour in field trials. We investigated whether iron (Fe) redox cycling could be the missing link needed to explain P dynamics in these systems. A pilot-scale DBR (Aotearoa New Zealand) was monitored for the first two drainage seasons (2017-2018), with supplemental in-field measurements of reduced solutes (Fe, HS/HS) and their conjugate oxidised species (Fe/SO) made in 2021 to constrain within-reactor redox gradients. Consistent with thermodynamics, the dissolution of Fe to Fe within the DBR sequentially followed O, NO and MnO reduction, but occurred before SO reduction. Monitoring of inlet and outlet chemistry revealed tight coupling between Fe and P (inlet R 0.94, outlet R 0.85), but distinct dynamics between drainage seasons. In season one, outlet P exceeded inlet P (net P source), and coincided with elevated outlet Fe, but at ⁓50 % lower P concentrations relative to inlet Fe:P ratios. In season 2 the reactor became a net P sink, coinciding with declining outlet Fe concentrations (indicating exhaustion of Fe hydroxides and associated P). In order to characterize P removal under varying source dynamics (i.e. inflows vs in-situ P releases), we used the inlet Fe vs P relationship to estimate P binding to colloidal Fe (hydr)oxide surfaces under oxic conditions, and the outlet Fe concentration to estimate in-situ P releases associated with Fe (hydr)oxide reduction. Inferred P-removal rates were highest early in season 1 (k = 0.60 g P m d; 75-100 % removal), declining significantly thereafter (k = 0.01 ± 0.02 g P m d; ca. 3-67 % removal). These calculations suggest that microbiological P removal in DBRs can occur at comparable magnitudes to nitrate removal by denitrification, depending mainly on P availability and hydraulic retention efficiency.

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http://dx.doi.org/10.1016/j.scitotenv.2024.170478DOI Listing

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